CN116952224A - Adaptive inertia/geomagnetic integrated navigation method based on geomagnetic chart suitability evaluation - Google Patents
Adaptive inertia/geomagnetic integrated navigation method based on geomagnetic chart suitability evaluation Download PDFInfo
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Abstract
本发明公开了一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法,根据地磁基准图的适配性评估算法,对该匹配区域内的地磁匹配适配性进行评价,根据评价结果自适应改变组合导航滤波器的参数或周期,以提高组合导航系统的精度。解决了地磁匹配算法对匹配区域内的地磁场的变化程度较为敏感,在适配性较低的区域地磁匹配算法的精度可能会下降,甚至出现无法匹配的情况,严重影响组合导航系统的精度的问题。
The invention discloses an adaptive inertial/geomagnetic combined navigation method based on geomagnetic map suitability evaluation. According to the suitability evaluation algorithm of the geomagnetic reference map, the geomagnetic matching suitability in the matching area is evaluated. According to the evaluation As a result, the parameters or periods of the integrated navigation filter are adaptively changed to improve the accuracy of the integrated navigation system. It solves the problem that the geomagnetic matching algorithm is sensitive to changes in the geomagnetic field in the matching area. In areas with low adaptability, the accuracy of the geomagnetic matching algorithm may decrease, or even fail to match, seriously affecting the accuracy of the integrated navigation system. question.
Description
技术领域Technical field
本发明涉及地磁导航领域,具体涉及一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法。The present invention relates to the field of geomagnetic navigation, and in particular to an adaptive inertial/geomagnetic combined navigation method based on geomagnetic map suitability evaluation.
背景技术Background technique
地磁导航系统是一种完全自主的导航手段,具有误差不随时间积累的优点,可以增强惯性导航系统,惯性/地磁组合导航系统可以提高导航系统整体性能。组合导航系统采用两种或两种以上导航系统对同一导航信息进行量测并且解算以形成量测量,从这些量测量中计算出导航系统的误差并进行校正。传统的惯性/地磁组合导航系统的工作流程为:首先根据规划好航迹区域的地磁信息选择合适的地磁分量制作地磁基准图,将绘制好的地磁基准图存储在载体飞行器的计算机中,由安装在飞行器上的地磁传感器实时获取该区域的匹配特征量的值。同时根据载体上的惯性导航系统(INS)输出的参考航迹,选取合适大小的匹配区域,进行地磁匹配,将结果与INS的输出结果进行滤波融合得到惯性/地磁组合导航系统的输出。由于地磁匹配算法对匹配区域内的地磁场的变化程度较为敏感,例如在某些地磁图自相似程度较高或者地图数值变化比较平缓的地区,地磁匹配算法的精度可能会下降,甚至出现无法匹配的情况,严重影响组合导航系统的精度。The geomagnetic navigation system is a completely autonomous navigation method. It has the advantage that errors do not accumulate over time. It can enhance the inertial navigation system. The inertial/geomagnetic combined navigation system can improve the overall performance of the navigation system. The integrated navigation system uses two or more navigation systems to measure and solve the same navigation information to form quantitative measurements. From these quantitative measurements, the navigation system errors are calculated and corrected. The workflow of the traditional inertial/geomagnetic integrated navigation system is as follows: first, select appropriate geomagnetic components based on the geomagnetic information of the planned track area to make a geomagnetic reference map, and store the drawn geomagnetic reference map in the computer of the carrier aircraft. The geomagnetic sensor on the aircraft obtains the value of the matching characteristic quantity in the area in real time. At the same time, according to the reference track output by the inertial navigation system (INS) on the carrier, a matching area of appropriate size is selected, geomagnetic matching is performed, and the result is filtered and fused with the output of the INS to obtain the output of the inertial/geomagnetic integrated navigation system. Since the geomagnetic matching algorithm is more sensitive to changes in the geomagnetic field within the matching area, for example, in areas where the degree of self-similarity of the geomagnetic map is high or the map value changes relatively slowly, the accuracy of the geomagnetic matching algorithm may decrease or even fail to match. situation, seriously affecting the accuracy of the integrated navigation system.
发明内容Contents of the invention
针对现有技术中的上述不足,本发明提供了一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法。In view of the above-mentioned deficiencies in the prior art, the present invention provides an adaptive inertial/geomagnetic integrated navigation method based on geomagnetic map suitability assessment.
为了达到上述发明目的,本发明采用的技术方案为:In order to achieve the above-mentioned object of the invention, the technical solutions adopted by the present invention are:
一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法,包括如下步骤:An adaptive inertial/geomagnetic integrated navigation method based on geomagnetic map suitability assessment, including the following steps:
S1、给定卡尔曼滤波器初始状态方程X0、初始协方差矩阵P0、初始系统噪声序列的方差矩阵Q0和初始量测噪声序列的方差矩阵R0;S1. Given the Kalman filter initial state equation X 0 , initial covariance matrix P 0 , variance matrix Q 0 of the initial system noise sequence and variance matrix R 0 of the initial measurement noise sequence;
S2、当卡尔曼滤波器与惯性导航解算周期同频率时进行时间更新,得到k时刻的状态估计值Xk和协方差矩阵Pk;S2. When the Kalman filter has the same frequency as the inertial navigation solution cycle, the time is updated to obtain the state estimate X k and covariance matrix P k at time k;
S3、当量测更新周期到来时获取地磁传感器量测值,并根据当前时刻的惯性导航参考位置提取匹配区域内的地磁图,根据所获取的地磁图计算粗糙方差比;S3. When the measurement update cycle arrives, obtain the geomagnetic sensor measurement value, extract the geomagnetic map in the matching area based on the inertial navigation reference position at the current moment, and calculate the rough variance ratio based on the obtained geomagnetic map;
S4、根据计算所得到的粗糙方差比进行卡尔曼滤波器参数自适应更新,若粗糙方差比小于设定阈值则该周期内不进行地磁匹配,若粗糙方差比大于等于设定阈值则通过地磁图适应性修正量测噪声序列的方差阵;S4. Adaptively update the Kalman filter parameters according to the calculated rough variance ratio. If the rough variance ratio is less than the set threshold, no geomagnetic matching will be performed in this period. If the rough variance ratio is greater than or equal to the set threshold, the geomagnetic map will be passed. Adaptively correct the variance matrix of the measurement noise sequence;
S5、根据地磁匹配输出的定位信息与惯性导航输出的参考位置获取k时刻的观测量并进行卡尔曼滤波器量测方程更新,根据量测更新结果校正惯性导航误差。S5. Obtain the observation at time k based on the positioning information output by geomagnetic matching and the reference position output by inertial navigation, update the Kalman filter measurement equation, and correct the inertial navigation error based on the measurement update results.
进一步的,所述S1中卡尔曼滤波器的状态方程表示为:Further, the state equation of the Kalman filter in S1 is expressed as:
其中,X(t)为t时刻以地理坐标系为导航坐标系建立的系统误差状态变量且Among them, X(t) is the system error state variable established using the geographical coordinate system as the navigation coordinate system at time t, and
式中,φE,φN,φU为捷联惯导数学平台姿态误差角分量,δvE,δvN,δvU为东北天向速度误差分量,依次为经度、纬度、高度误差,εbx,εby,εbz一次为陀螺常值漂移误差三轴分量,/>为加速度计零偏;In the formula, φ E , φ N , φ U are the attitude error angular components of the strapdown inertial navigation mathematical platform, δv E , δv N , δv U are the northeast direction velocity error components, are the longitude, latitude, and altitude errors in sequence, ε bx , ε by , and ε bz are once the three-axis component of the gyro constant drift error, /> is the accelerometer zero bias;
F(t)为系统状态转移矩阵:F(t) is the system state transition matrix:
式中,FN为对应的9维基本导航参数系统阵,FS为惯性器件误差与姿态速度位置误差之间的状态转移矩阵,FM为惯性器件误差自身的状态转移矩阵且In the formula, F N is the corresponding 9-dimensional basic navigation parameter system array, F S is the state transfer matrix between the inertial device error and the attitude speed position error, F M is the state transfer matrix of the inertial device error itself, and
FM=[06×6]F M =[0 6×6 ]
为弹体坐标系b到导航坐标系n的坐标转换矩阵; is the coordinate transformation matrix from the missile coordinate system b to the navigation coordinate system n;
G(t)为系统噪声转移矩阵且G(t) is the system noise transfer matrix and
W(t)为系统白噪声误差矩阵且W(t) is the system white noise error matrix and
式中,为陀螺仪随机误差的三轴分量,/>为加速度计的随机误差的三轴分量。In the formula, is the three-axis component of the gyroscope’s random error,/> is the three-axis component of the accelerometer’s random error.
进一步的,所述S3中粗糙方差比的具体计算方式为:Further, the specific calculation method of the rough variance ratio in S3 is:
ξ=R/σm ξ=R/σ m
其中,ξ为粗糙方差比,R为地磁变化粗糙度且Among them, ξ is the roughness variance ratio, R is the geomagnetic variation roughness and
R=(Rx+Ry)/2R=(R x +R y )/2
式中,Rx、Ry为地磁变化粗糙度对应方向上的分量,m和n为被评估区域的地磁图大小为m×n,M(i,j)为地磁图中编号为(i,j)的网格的地磁强度值;In the formula, R x and R y are the components in the corresponding directions of the geomagnetic variation roughness, m and n are the geomagnetic map size of the evaluated area, which is m×n, and M(i, j) is the geomagnetic map numbered (i, j) The geomagnetic intensity value of the grid;
σm为地磁强度值标准差且σ m is the standard deviation of geomagnetic intensity values and
式中,Em为区域内地磁强度值的平均值且In the formula, E m is the average value of geomagnetic intensity in the area and
进一步的,所述S4中卡尔曼滤波器参数自适应更新的具体方式为:Further, the specific method of adaptively updating the Kalman filter parameters in S4 is:
其中,Rk为k时刻的量测噪声序列的方差阵,ξ为粗糙方差比。Among them, R k is the variance matrix of the measurement noise sequence at time k, and ξ is the rough variance ratio.
进一步的,所述S5中根据地磁匹配输出的定位信息与惯性导航输出的参考位置获取k时刻的观测量表示为:Further, in S5, the observation quantity at time k obtained based on the positioning information output by geomagnetic matching and the reference position output by inertial navigation is expressed as:
其中,Z为量测量,依次为经度、纬度和高度的误差,/>依次为捷联惯导输出的经度、纬度和高度信息,λm、/>为地磁匹配输出的经度和纬度信息,hm是气压高度计输出的临近空间高超声速飞行器的高度。Among them, Z is the quantity measurement, Errors in longitude, latitude and altitude, in order,/> The longitude, latitude and altitude information output by strapdown inertial navigation are in sequence, λ m ,/> is the longitude and latitude information output by geomagnetic matching, h m is the altitude of the nearby space hypersonic aircraft output by the barometric altimeter.
进一步的,所述S5中卡尔曼滤波器量测方程更新的具体方式为:Further, the specific method for updating the Kalman filter measurement equation in S5 is:
S51、对状态方程离散化,根据初始状态进行状态一步预测 S51. Discretize the state equation and perform one-step prediction of the state based on the initial state.
其中,为k-1时刻状态矢量的收敛值;in, is the convergence value of the state vector at time k-1;
S52、利用一步预测值进行状态估计:S52. Use one-step prediction value for state estimation:
其中,Kk为滤波增益矩阵;Among them, K k is the filter gain matrix;
其中,Rk为k时刻量测噪声的协方差阵,Pk/k-1为一步预测均方误差阵,其对角线元素是各个状态估计的方差;Among them, R k is the covariance matrix of the measurement noise at time k, P k/k-1 is the one-step prediction mean square error matrix, and its diagonal elements are the variances of each state estimate;
其中,Qk-1为k-1时刻系统噪声的协方差阵,Pk-1为k-1时刻估计均方误差矩阵,k时刻估计均方误差矩阵Pk为Among them, Q k-1 is the covariance matrix of the system noise at time k-1, P k-1 is the estimated mean square error matrix at time k-1, and the estimated mean square error matrix at time k P k is
其中,I为单位阵;Among them, I is the unit matrix;
S53、给定初值X0和P0,根据k时刻的位置量测矢量Zk,递推求得k时刻的状态估计 S53. Given the initial values X 0 and P 0 , according to the position measurement vector Z k at time k, recursively obtain the state estimate at time k.
S54、经过重复计算n次得到的收敛值。S54. After repeated calculation n times, we get convergence value.
本发明具有以下有益效果:The invention has the following beneficial effects:
根据地磁基准图的适配性评估算法,对该匹配区域内的地磁匹配适配性进行评价,根据评价结果自适应改变组合导航滤波器的参数或周期,以提高组合导航系统的精度。According to the suitability evaluation algorithm of the geomagnetic reference map, the geomagnetic matching suitability in the matching area is evaluated, and the parameters or periods of the integrated navigation filter are adaptively changed according to the evaluation results to improve the accuracy of the integrated navigation system.
附图说明Description of the drawings
图1为本发明一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法流程示意图。Figure 1 is a schematic flowchart of an adaptive inertial/geomagnetic combined navigation method based on geomagnetic map suitability assessment according to the present invention.
具体实施方式Detailed ways
下面对本发明的具体实施方式进行描述,以便于本技术领域的技术人员理解本发明,但应该清楚,本发明不限于具体实施方式的范围,对本技术领域的普通技术人员来讲,只要各种变化在所附的权利要求限定和确定的本发明的精神和范围内,这些变化是显而易见的,一切利用本发明构思的发明创造均在保护之列。The specific embodiments of the present invention are described below to facilitate those skilled in the art to understand the present invention. However, it should be clear that the present invention is not limited to the scope of the specific embodiments. For those of ordinary skill in the technical field, as long as various changes These changes are obvious within the spirit and scope of the invention as defined and determined by the appended claims, and all inventions and creations utilizing the concept of the invention are protected.
一种基于地磁图适配性评估的自适应惯性/地磁组合导航方法,如图1所示,包括如下步骤:An adaptive inertial/geomagnetic integrated navigation method based on geomagnetic map suitability assessment, as shown in Figure 1, includes the following steps:
S1、给定卡尔曼滤波器初始状态方程X0、初始协方差矩阵P0、初始系统噪声序列的方差矩阵Q0和初始量测噪声序列的方差矩阵R0;S1. Given the Kalman filter initial state equation X 0 , initial covariance matrix P 0 , variance matrix Q 0 of the initial system noise sequence and variance matrix R 0 of the initial measurement noise sequence;
卡尔曼滤波器的状态方程表示为:The state equation of the Kalman filter is expressed as:
其中,X(t)为t时刻以地理坐标系为导航坐标系建立的系统误差状态变量且Among them, X(t) is the system error state variable established using the geographical coordinate system as the navigation coordinate system at time t, and
式中,φE,φN,φU为捷联惯导数学平台姿态误差角分量,δvE,δvN,δvU为东北天向速度误差分量,依次为经度、纬度、高度误差,εbx,εby,εbz一次为陀螺常值漂移误差三轴分量,/>为加速度计零偏;In the formula, φ E , φ N , φ U are the attitude error angular components of the strapdown inertial navigation mathematical platform, δv E , δv N , δv U are the northeast direction velocity error components, are the longitude, latitude, and altitude errors in sequence, ε bx , ε by , ε bz is once the three-axis component of the gyro constant drift error, /> is the accelerometer zero bias;
F(t)为系统状态转移矩阵:F(t) is the system state transition matrix:
式中,FN为对应的9维基本导航参数系统阵,FS为惯性器件误差与姿态速度位置误差之间的状态转移矩阵,FM为惯性器件误差自身的状态转移矩且In the formula, F N is the corresponding 9-dimensional basic navigation parameter system array, F S is the state transfer matrix between the inertial device error and the attitude speed position error, F M is the state transfer moment of the inertial device error itself, and
FM=[06×6] (5)F M =[0 6×6 ] (5)
G(t)为系统噪声转移矩阵且G(t) is the system noise transfer matrix and
为弹体坐标系b到导航坐标系n的坐标转换矩阵; is the coordinate transformation matrix from the missile coordinate system b to the navigation coordinate system n;
W(t)为系统白噪声误差矩阵且W(t) is the system white noise error matrix and
式中,为陀螺仪随机误差的三轴分量,/>为加速度计的随机误差的三轴分量。In the formula, is the three-axis component of the gyroscope’s random error,/> is the three-axis component of the accelerometer’s random error.
系统的观测方程可表示为:The observation equation of the system can be expressed as:
Z(t)=H(t)X(t)+V(t) (8)Z(t)=H(t)X(t)+V(t) (8)
由于地磁匹配输出的位置为水平位置,不含高度信息,这样就无法对INS的高度误差进行有效的修正,故在高度通道引入气压高度计来输出高度信息修正SINS系统的高度误差。Since the geomagnetic matching output position is a horizontal position and does not contain altitude information, the altitude error of the INS cannot be effectively corrected. Therefore, a barometric altimeter is introduced into the altitude channel to output altitude information to correct the altitude error of the SINS system.
S2、当卡尔曼滤波器与惯性导航解算周期同频率时进行时间更新,得到k时刻的状态估计值Xk和协方差矩阵Pk;S2. When the Kalman filter has the same frequency as the inertial navigation solution cycle, the time is updated to obtain the state estimate X k and covariance matrix P k at time k;
S3、当量测更新周期到来时获取地磁传感器量测值,并根据当前时刻的惯性导航参考位置提取匹配区域内的地磁图,根据所获取的地磁图计算粗糙方差比;S3. When the measurement update cycle arrives, obtain the geomagnetic sensor measurement value, extract the geomagnetic map in the matching area based on the inertial navigation reference position at the current moment, and calculate the rough variance ratio based on the obtained geomagnetic map;
地磁图适配性评估有若干个指标,其中比较有代表性的是粗糙方差比。地磁强度值标准差,可以反映地磁背景场的起伏变化,方差越大,地磁图起伏越大,匹配可靠性越强,反之,匹配可靠性越差。地磁强度值标准差如下所示:There are several indicators for evaluating the suitability of geomagnetic maps, among which the more representative one is the rough variance ratio. The standard deviation of geomagnetic intensity values can reflect the fluctuations of the geomagnetic background field. The greater the variance, the greater the fluctuations of the geomagnetic map, and the stronger the matching reliability. On the contrary, the worse the matching reliability. The standard deviation of geomagnetic intensity values is as follows:
式中,m和n表示被评估区域的地磁图大小为m×n,M(i,j)表示地磁图中编号为(i,j)的网格的地磁强度值,Em是区域内地磁强度值的平均值:In the formula, m and n represent that the size of the geomagnetic map in the assessed area is m×n, M(i,j) represents the geomagnetic intensity value of the grid numbered (i,j) in the geomagnetic map, and E m is the geomagnetic intensity in the area. Average intensity value:
粗糙度是指地磁背景场表面具有的较小的间距和微小的峰谷所组成的微观几何形状特征,地磁变化粗糙程度越大,表面特征越明显,越有利于导航。粗糙度R的计算由式(13)给出:Roughness refers to the microscopic geometric shape characteristics composed of small spacing and tiny peaks and valleys on the surface of the geomagnetic background field. The greater the roughness of the geomagnetic change, the more obvious the surface features are, and the more conducive it is to navigation. The calculation of roughness R is given by equation (13):
R=(Rx+Ry)/2 (13)R=(R x +R y )/2 (13)
粗糙方差比表示相邻采样点见变化比的大小,定义为:The rough variance ratio represents the change ratio of adjacent sampling points, and is defined as:
ξ=R/σm (14)ξ=R/σ m (14)
比值小表示采样点间变化较小,但整个区域可能有较大而缓慢的起伏,地磁值变化比较平滑。而比值大则表示相邻采样点之间的变化比整个区域的起伏相对更大,因此越容易实现地磁匹配,本方法使用粗糙方差ξ比作为地磁图适配性评估的依据,并通过ξ对组合导航系统中的Rk阵进行修正。A small ratio means that the changes between sampling points are small, but the entire area may have large and slow fluctuations, and the geomagnetic value changes relatively smoothly. A large ratio means that the changes between adjacent sampling points are relatively larger than the fluctuations of the entire area, so it is easier to achieve geomagnetic matching. This method uses the rough variance ξ ratio as the basis for evaluating the suitability of the geomagnetic map, and uses ξ to The R k matrix in the integrated navigation system is corrected.
S4、根据计算所得到的粗糙方差比进行卡尔曼滤波器参数自适应更新,若粗糙方差比小于设定阈值则该周期内不进行地磁匹配,若粗糙方差比大于等于设定阈值则通过地磁图适应性修正量测噪声序列的方差阵;S4. Adaptively update the Kalman filter parameters according to the calculated rough variance ratio. If the rough variance ratio is less than the set threshold, no geomagnetic matching will be performed in this period. If the rough variance ratio is greater than or equal to the set threshold, the geomagnetic map will be passed. Adaptively correct the variance matrix of the measurement noise sequence;
卡尔曼滤波观测方程的量测量Z由INS输出的水平位置信息与地磁匹配输出的水平位置之差Z1和SINS输出的高度信息与高度计输出的高度信息之差Z2两部分组成。Z1和Z2的定义如下:The quantity measurement Z of the Kalman filter observation equation consists of the difference Z 1 between the horizontal position information output by the INS and the geomagnetic matching output, and the difference Z 2 between the altitude information output by the SINS and the altitude information output by the altimeter. Z 1 and Z 2 are defined as follows:
Z2=[hs-hm] (16)Z 2 =[h s -h m ] (16)
式(15)和(16)中,分别为SINS输出的经纬高信息;/>为地磁匹配输出的经纬度信息;hm是气压高度计输出的临近空间高超声速飞行器的高度。故In formulas (15) and (16), They are the longitude, latitude and height information output by SINS;/> is the latitude and longitude information output by geomagnetic matching; h m is the altitude of the nearby space hypersonic aircraft output by the barometric altimeter. Therefore
式(8)中H()为观测矩阵In formula (8), H() is the observation matrix
H(t)=[H11 H12 H13 H14 H15]T (18)H(t)=[H 11 H 12 H 13 H 14 H 15 ] T (18)
上式中矩阵的各个分量表达式为The expressions of each component of the matrix in the above formula are
H11=H13=H14=H15=03×3 (19)H 11 =H 13 =H 14 =H 15 =0 3×3 (19)
V()为地磁匹配的观测噪声矩阵。由于V() is the observation noise matrix of geomagnetic matching. because
因此,therefore,
S5、根据地磁匹配输出的定位信息与惯性导航输出的参考位置获取k时刻的观测量并进行卡尔曼滤波器量测方程更新,根据量测更新结果校正惯性导航误差。S5. Obtain the observation at time k based on the positioning information output by geomagnetic matching and the reference position output by inertial navigation, update the Kalman filter measurement equation, and correct the inertial navigation error based on the measurement update results.
对状态方程式(1)离散化后,设tk时刻的被估计状态Xk受到系统噪声Wk-1驱动,驱动机理由下述状态方程描述After discretizing the state equation (1), assume that the estimated state X k at time t k is driven by the system noise W k-1 . The driving mechanism is described by the following state equation.
Xk=Φk,k-1Xk-1+Γk-1WK-1 (22)X k =Φ k,k-1 X k-1 +Γ k-1 W K-1 (22)
量测方程为The measurement equation is
Zk=HkXk+Vk (23) Zk = HkXk + Vk (23)
其中,Φk,k-1为tk-1时刻的一步转移矩阵,Γk-1为系统噪声驱动阵,Wk是系统噪声,一般认为是白噪声;Hk为量测矩阵,Vk为量测噪声;同时Wk和Vk满足Among them, Φ k, k-1 is the one-step transfer matrix at time t k-1 , Γ k-1 is the system noise driving matrix, W k is the system noise, generally considered to be white noise; H k is the measurement matrix, V k is the measurement noise; at the same time, W k and V k satisfy
其中,Qk为系统噪声序列的方差阵;Rk为量测噪声序列的方差阵。Among them, Q k is the variance matrix of the system noise sequence; R k is the variance matrix of the measurement noise sequence.
如果被估计量Xk满足式(22),对Xk的量测Zk满足式(23),系统噪声Wk和量测噪声Vk满足式(24),系统噪声方差阵Qk非负定,量测噪声序列的方差阵Rk正定,通过地磁图适配性评价ξ进行修正: If the estimator X k satisfies equation ( 22) , the measurement Z k of Definite, the variance matrix R k of the measurement noise sequence is positive definite, and is corrected through the geomagnetic map suitability evaluation ξ:
卡尔曼滤波器量测方程更新的具体方式为:The specific way to update the Kalman filter measurement equation is:
S51、对状态方程离散化,根据初始状态进行状态一步预测 S51. Discretize the state equation and perform one-step prediction of the state based on the initial state.
其中,为k-1时刻状态矢量的收敛值;in, is the convergence value of the state vector at time k-1;
S52、利用一步预测值进行状态估计:S52. Use one-step prediction value for state estimation:
其中,Kk为滤波增益矩阵;Among them, K k is the filter gain matrix;
其中,Rk为k时刻量测噪声的协方差阵,Pk/k-1为一步预测均方误差阵,其对角线元素是各个状态估计的方差;Among them, R k is the covariance matrix of the measurement noise at time k, P k/k-1 is the one-step prediction mean square error matrix, and its diagonal elements are the variances of each state estimate;
其中,Qk-1为k-1时刻系统噪声的协方差阵,Pk-1为k-1时刻估计均方误差矩阵,k时刻估计均方误差矩阵Pk为Among them, Q k-1 is the covariance matrix of the system noise at time k-1, P k-1 is the estimated mean square error matrix at time k-1, and the estimated mean square error matrix at time k P k is
其中,I为单位阵;Among them, I is the unit matrix;
S53、给定初值X0和P0,根据k时刻的位置量测矢量Zk,递推求得k时刻的状态估计 S53. Given the initial values X 0 and P 0 , according to the position measurement vector Z k at time k, recursively obtain the state estimate at time k.
S54、经过重复计算n次得到的收敛值。S54. After repeated calculation n times, we get convergence value.
本发明中应用了具体实施例对本发明的原理及实施方式进行了阐述,以上实施例的说明只是用于帮助理解本发明的方法及其核心思想;同时,对于本领域的一般技术人员,依据本发明的思想,在具体实施方式及应用范围上均会有改变之处,综上所述,本说明书内容不应理解为对本发明的限制。The present invention uses specific embodiments to illustrate the principles and implementation methods of the present invention. The description of the above embodiments is only used to help understand the method of the present invention and its core idea; at the same time, for those of ordinary skill in the art, based on this The idea of the invention will be subject to change in the specific implementation and scope of application. In summary, the contents of this description should not be understood as limiting the invention.
本领域的普通技术人员将会意识到,这里所述的实施例是为了帮助读者理解本发明的原理,应被理解为本发明的保护范围并不局限于这样的特别陈述和实施例。本领域的普通技术人员可以根据本发明公开的这些技术启示做出各种不脱离本发明实质的其它各种具体变形和组合,这些变形和组合仍然在本发明的保护范围内。Those of ordinary skill in the art will appreciate that the embodiments described here are provided to help readers understand the principles of the present invention, and it should be understood that the scope of the present invention is not limited to such specific statements and embodiments. Those of ordinary skill in the art can make various other specific modifications and combinations based on the technical teachings disclosed in the present invention without departing from the essence of the present invention, and these modifications and combinations are still within the protection scope of the present invention.
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